3  Effect of stream and year on the somatic-to-otolith size relationship of Juvenile Brook Trout (Salvelinus fontinalis).

Author

Michael J Hayden, and Mike Akresh, Ph.D.

4 Introduction

Otoliths are tiny, calcified structures found in a fish’s head that aid orientation and hearing (Campana and Neilson 1985). In addition to their biological role, Otoliths serve as valuable resources for fisheries biologists and managers, enabling them to reconstruct the life history of individual fish. When viewed under a microscope, the otolith looks like a tree stump with individual rings corresponding to the years the fish has been alive. Upon closer inspection, one notices that the large yearly rings are composed of smaller daily rings. Both yearly and daily rings allow managers and scientists to gather information on birth date (Campana and Neilson 1985), environmental water chemistry (Høie, Otterlei, and Folkvord 2004; Radtke et al. 1996), metabolic rate, and even size at age estimates [ Ashworth (2017) ; Campana (1990) ; Vigliola and Meekan (2009)]. Size at age estimates is valuable information because they have many applications. For example, knowing cod’s otolith age/size relationship can prohibit fishermen from harvesting the most fecund age/size class in this species. (Høie, Otterlei, and Folkvord 2004; Anderson, Claiborne, and Smith 2023)

Although back-calculation is widely used to estimate past sizes at a given age, three assumptions must be met. First, an annual or daily rate of ring deposition that does not vary; second, increments can be read precisely and accurately; and third, a relationship between increment spacing and somatic growth is usually measured in body size (Campana 1990; Vigliola and Meekan 2009). The first two assumptions are met through ring formation rate and reader evaluations; however, the third requires further analysis because of the possibility of somatic growth uncoupling from otolith ring deposition, leading to either underestimation or overestimating body size (Campana 1990; Vigliola and Meekan 2009). This can happen either because of a “growth effect,” where the otolith of slow-growing fish is larger at a given size than that of fast-growing fish, or an “age effect,” where the deposition of daily rings occurs despite fluctuations in somatic growth (Vigliola and Meekan 2009). Therefore, a way to overcome this needs to be established [(Covich, Crowl, and Heartsill-Scalley 2006)

Several methodologies have been used to account for the age and growth effect of the relationship between otolith and fish size. The Frasher Lee methodology attempted to account for the age/growth effect by assuming that if the otolith was 10% larger than the mean size, the fish must be 10% larger than the others [Vigliola and Meekan (2009)][.] Campana (1990) introduced a modification known as the biological intercept method, which posited that the fish had a specific size when the otolith measured zero, which was integrated with the proportionality concept of the Frasher-Lee equation. Additionally, other methods have utilized temperature to clarify the relationship (Mosegaard, Svedäng, and Taberman 1988; Shafer 2000). Using developmental temperature as a proxy; I propose to build upon past work and test the relationship between juvenile brook trout otolith and fish size.

4.1 Questions

  • Is there a linear relationship between Brook Trout YOY body size measured in fork length (mm) and otolith radius (um)?

  • With the addition of stream and year sampled covariates, can we make better Fork Length predictions using measured Otolith Radius (um)

5 Methods

5.1 Variables

  • Fork Length - Continuous Response

  • Otolith Radius - Continuous Predictor

  • Stream - Categorical Predictor (Covariate)

  • Year Sampled (Cohort) - Categorical Predictor (Covariate)

5.2 Data Collection

5.2.1 Field

5.2.2 Lab (Otolith Analysis)

  • A sagittal otolith is divided into four quadrants.
    1. Posterior-Ventral
    2. Posterior-Dorsal
    3. Anterior-Ventral
    4. Anterior-Dorsal

Posterior-Dorsal Quadrant with Counting Line
  • Otolith Radius was measured along a 45 degree angle in the Posterior-Dorsal Quadrant
    • Starting at the Posterior most primordia of the primordium.
    • Ending at the edge of the Otolith.

5.3 Data Analysis

5.3.1 Graphs

  • Density plot of otolith radius is a gamma distribution because it is rightly skewed, non negative interegers and non

Code
streamFishOtolithKey %>% select(river, yearSampled, radius) %>% na.omit() %>% group_by(yearSampled) %>% summarise( count = n() )
# A tibble: 2 × 2
  yearSampled count
        <dbl> <int>
1        2014   153
2        2015   156
Code
streamFishOtolithKey %>% select(river, yearSampled, radius) %>% na.omit() %>% group_by( river) %>% summarise( count = n() )
# A tibble: 5 × 2
  river              count
  <chr>              <int>
1 Obear Brook           63
2 Pond Brook            53
3 Roaring Brook         76
4 Sanderson Brook       37
5 West Whately Brook    80

5.4 Model Assumptions

p value > 0.05, some col linearity in the data


    Fisher's Exact Test for Count Data with simulated p-value (based on
    10000 replicates)

data:  t_soil_vil
p-value = 0.0021
alternative hypothesis: two.sided

5.5 Model Fitting

  • Model Assumptions of Collinearity and Linearity were met.

  • I will use a gamma distribution because density plots indicate data is non-negative, rightly skewed and non-integers.

5.5.1 Linear Regression


Call:
glm(formula = forkLength ~ radius, family = Gamma(link = "log"), 
    data = streamFishOtolithKey)

Coefficients:
             Estimate Std. Error t value Pr(>|t|)    
(Intercept) 2.883e+00  2.000e-02  144.12   <2e-16 ***
radius      2.486e-03  5.109e-05   48.66   <2e-16 ***
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

(Dispersion parameter for Gamma family taken to be 0.0247221)

    Null deviance: 63.3337  on 308  degrees of freedom
Residual deviance:  7.4672  on 307  degrees of freedom
  (387 observations deleted due to missingness)
AIC: 2045.7

Number of Fisher Scoring iterations: 4


Call:
lm(formula = forkLength ~ radius * river * yearSampled, data = streamNew)

Residuals:
     Min       1Q   Median       3Q      Max 
-18.7417  -3.7079  -0.2308   3.3127  19.2968 

Coefficients:
                                             Estimate Std. Error t value
(Intercept)                                -3.145e+03  6.588e+03  -0.477
radius                                      4.527e+00  1.703e+01   0.266
riverWest Whately Brook                    -2.259e+04  1.257e+04  -1.797
yearSampled                                 1.565e+00  3.271e+00   0.478
radius:riverWest Whately Brook              5.288e+01  3.160e+01   1.674
radius:yearSampled                         -2.189e-03  8.455e-03  -0.259
riverWest Whately Brook:yearSampled         1.122e+01  6.242e+00   1.797
radius:riverWest Whately Brook:yearSampled -2.626e-02  1.569e-02  -1.674
                                           Pr(>|t|)  
(Intercept)                                  0.6338  
radius                                       0.7908  
riverWest Whately Brook                      0.0744 .
yearSampled                                  0.6330  
radius:riverWest Whately Brook               0.0963 .
radius:yearSampled                           0.7961  
riverWest Whately Brook:yearSampled          0.0744 .
radius:riverWest Whately Brook:yearSampled   0.0962 .
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

Residual standard error: 6.2 on 148 degrees of freedom
  (164 observations deleted due to missingness)
Multiple R-squared:  0.9074,    Adjusted R-squared:  0.903 
F-statistic: 207.2 on 7 and 148 DF,  p-value: < 2.2e-16
  • Little difference between Standard Error and the intercept.

  • R Sqared value did not change between General Linear Model and General Additive Models.

Interpretation

  • Generalized Linear Model

5.5.2 Mixed Effects Model

Generalized linear mixed model fit by maximum likelihood (Laplace
  Approximation) [glmerMod]
 Family: Gamma  ( log )
Formula: forkLength ~ radius + (1 | yearSampled) + (1 | river)
   Data: streamFishOtolithKey

     AIC      BIC   logLik deviance df.resid 
  2023.1   2041.7  -1006.5   2013.1      304 

Scaled residuals: 
     Min       1Q   Median       3Q      Max 
-2.43511 -0.69850 -0.08442  0.67797  3.01237 

Random effects:
 Groups      Name        Variance  Std.Dev.
 river       (Intercept) 0.0002817 0.01678 
 yearSampled (Intercept) 0.0007034 0.02652 
 Residual                0.0220464 0.14848 
Number of obs: 309, groups:  river, 5; yearSampled, 2

Fixed effects:
             Estimate Std. Error t value Pr(>|z|)    
(Intercept) 2.917e+00  5.619e-02   51.91   <2e-16 ***
radius      2.381e-03  5.461e-05   43.60   <2e-16 ***
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

Correlation of Fixed Effects:
       (Intr)
radius -0.339
optimizer (Nelder_Mead) convergence code: 0 (OK)
Model failed to converge with max|grad| = 0.00560503 (tol = 0.002, component 1)
Model is nearly unidentifiable: very large eigenvalue
 - Rescale variables?
Model is nearly unidentifiable: large eigenvalue ratio
 - Rescale variables?
                R2m       R2c
delta     0.8833392 0.8883292
lognormal 0.8844122 0.8894082
trigamma  0.8822452 0.8872290
# Intraclass Correlation Coefficient

    Adjusted ICC: 0.043
  Unadjusted ICC: 0.005

Generalized linear mixed model fit by maximum likelihood (Laplace
  Approximation) [glmerMod]
 Family: Gamma  ( log )
Formula: forkLength ~ radius + (1 | river)
   Data: streamFishOtolithKey

     AIC      BIC   logLik deviance df.resid 
    2044     2059    -1018     2036      305 

Scaled residuals: 
    Min      1Q  Median      3Q     Max 
-2.3189 -0.7145 -0.1843  0.6584  2.7865 

Random effects:
 Groups   Name        Variance  Std.Dev.
 river    (Intercept) 0.0004284 0.0207  
 Residual             0.0240138 0.1550  
Number of obs: 309, groups:  river, 5

Fixed effects:
             Estimate Std. Error t value Pr(>|z|)    
(Intercept) 2.880e+00  2.560e-02  112.50   <2e-16 ***
radius      2.491e-03  5.218e-05   47.74   <2e-16 ***
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

Correlation of Fixed Effects:
       (Intr)
radius -0.703
optimizer (Nelder_Mead) convergence code: 0 (OK)
Model failed to converge with max|grad| = 0.00829334 (tol = 0.002, component 1)
Model is nearly unidentifiable: very large eigenvalue
 - Rescale variables?
Model is nearly unidentifiable: large eigenvalue ratio
 - Rescale variables?
                R2m       R2c
delta     0.8864589 0.8884489
lognormal 0.8876291 0.8896217
trigamma  0.8852637 0.8872510

  • Both mixed models show minimal variance due to the random effects associated with each. This observation is clear when comparing the small residual values: 2.181 to 39.366.

5.5.3 Generalized Additive Model (GAM)


Family: gaussian 
Link function: identity 

Formula:
forkLength ~ s(radius)

Parametric coefficients:
            Estimate Std. Error t value Pr(>|t|)    
(Intercept)  46.6887     0.3385   137.9   <2e-16 ***
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

Approximate significance of smooth terms:
            edf Ref.df     F p-value    
s(radius) 6.491  7.647 441.2  <2e-16 ***
---
Signif. codes:  0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1

R-sq.(adj) =  0.916   Deviance explained = 91.8%
GCV = 36.276  Scale est. = 35.397    n = 309

Anderson, Austin J., Andrew M. Claiborne, and Wade Smith. 2023. “Validation of Age Estimates for Chum and Sockeye Salmon Derived from Otolith and Scale Analysis.” Fisheries Research 259 (March). https://doi.org/10.1016/j.fishres.2022.106556.
Ashworth, Eloïse C. 2017. “Exploration of the Relationship Between Somatic and Otolith Growth, and Development of a Proportionality-Based Back-Calculation Approach Based on Traditional Growth Equations.” https://www.researchgate.net/publication/317536602.
Campana, Steven E. 1990. “How Reliable Are Growth Back-Calculations Based on Otoliths?” Canadian Journal of Fisheries and Aquatic Sciences 47 (11): 2219–27. https://doi.org/10.1139/f90-246.
Campana, Steven E., and John Neilson. 1985. “Microstructure of Fish Otoliths. Can. 1. Fish.” Can. J. Fish. Aquat. Sci 42 (January): 1014–32. www.nrcresearchpress.com.
Covich, Alan P., Todd A. Crowl, and Tamara Heartsill-Scalley. 2006. “Effects of Drought and Hurricane Disturbances on Headwater Distributions of Palaemonid River Shrimp ( Macrobrachium Spp.) in the Luquillo Mountains, Puerto Rico.” Journal of the North American Benthological Society 25 (1): 99–107. https://doi.org/10.1899/0887-3593(2006)25[99:EODAHD]2.0.CO;2.
Høie, Hans, Erling Otterlei, and Arild Folkvord. 2004. “Temperature-Dependent Fractionation of Stable Oxygen Isotopes in Otoliths of Juvenile Cod (Gadus Morhua l.).” ICES Journal of Marine Science 61 (2): 243–51. https://doi.org/10.1016/j.icesjms.2003.11.006.
Mosegaard, Henrik, Henrik Svedäng, and Kjell Taberman. 1988. “Uncoupling of Somatic and Otolith Growth Rates in Arctic Char ( Salvelinus Alpinus) as an Effect of Differences in Temperature Response.” Canadian Journal of Fisheries and Aquatic Sciences 45 (9): 1514–24. https://doi.org/10.1139/f88-180.
Radtke, R L, W Showers, E Moksness, and P Lenz. 1996. “Environmental Information Stored in Otoliths: Insights from Stable Isotopes.” Marine Biology 127 (June): 170.
Shafer, D. J. 2000. “Evaluation of Periodic and Aperiodic Otolith Structure and Somatic-Otolith Scaling for Use in Retrospective Life History Analysis of a Tropical Marine Goby, Bathygobius Coalitus.” Marine Ecology Progress Series 199 (June): 217–29. https://doi.org/10.3354/meps199217.
Vigliola, Laurent, and Mark G. Meekan. 2009. “The Back-Calculation of Fish Growth from Otoliths.” In, 174–211. https://doi.org/10.1007/978-1-4020-5775-5_6.